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ERS186: Environmental Remote Sensing
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ERS186: Environmental Remote Sensing
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ERS186: Environmental Remote Sensing Lecture 9: Soils Overview Applications Soil Science Physical Principles Reflectance (specular and diffuse scattering) Absorption ...
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Species Discrimination Using Remote Sensing ... PROSPECT (Jacquemoud et al., 1996): models ... Greenberg et al. 2001, healthy and water stressed cotton spectra. ...
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Parallelepiped. Minimum distance. Maximum likelihood. Classifier Inputs ... Parallelepiped ... Parallelepiped. Minimum Distance ...
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Reflectance (specular and diffuse scattering) Absorption bands ... If a surface is smooth (particles smaller than wavelength), specular reflection is important. ...
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Pores can contain air or water (or ice! ... Water is a strong absorber, so soils with more moisture will be darker over most ... Water has a higher thermal ...
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... the onset of a strong wind, the irradiance on a deciduous forest floor increases ... RT models can be: ... invertible models: typically designed ...
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Most of geological remote sensing asks the following question: For a reflectance curve (spectrum) either determined in the lab, with a field ... Fresnel equation: ...
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Parallelepiped. Minimum distance. Maximum likelihood. Table Look Up ... Parallelepiped ... Parallelepiped. Minimum Distance ...
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